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    Comments on “The Effect of Changes in the Earth's Obliquity on the Distribution of Mean Annual Sea Level Temperatures” 

    Source: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 004:;page 839
    Author(s): Bowling, Sue Ann
    Publisher: American Meteorological Society
    Abstract: tract
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    Climatology of High-Latitude Air Pollution as Illustrated by Fairbanks and Anchorage, Alaska 

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 001:;page 22
    Author(s): Bowling, Sue Ann
    Publisher: American Meteorological Society
    Abstract: High latitude communities frequently have severe air pollution problems. The usual situation is the release of moderate amounts of pollutants into an atmosphere with extremely poor dispersion. The poor dispersion is in ...
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    Comments on “Cirrus Clouds and the Climate” 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 005:;page 1003
    Author(s): Bowling, Sue Ann
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Quasi-Equilibrium Temperature Differences between Radiating Ice Crystals and the Surrounding Air 

    Source: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 005:;page 991
    Author(s): Bowling, Sue Ann; Benson, Carl S.; Murcray, Wallace B.
    Publisher: American Meteorological Society
    Abstract: A previous attempt to calculate the temperature gradient around a growing ice crystal in clear air started with the radiation budget of the crystal plus the assumption that the measured frost point temperature (about 2C ...
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    Winter Pressure Systems and Ice Fog in Fairbanks, Alaska 

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 006:;page 961
    Author(s): Bowling, Sue Ann; Ohtake, Takeshi; Benson, Carl S.
    Publisher: American Meteorological Society
    Abstract: The production of the low temperatures which are responsible for ice fog in inhabited areas of interior Alaska would appear to be a classic example of clear sky radiative cooling under nearly polar night conditions. However, ...
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